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峰丛洼地石漠化区不同土地利用方式表层土壤持水能力研究

Water-holding capacity of surface soils of different land-use patterns in the rocky desertification area of the peak cluster depression

  • 摘要: 以3种自然生态系统(撂荒地、灌草地、自然林)和4种人工生态系统(人工林、玉米地、核桃林、猕猴桃)土地利用方式为研究对象,通过测定土壤持水指标和土壤性质,探析峰丛洼地石漠化区不同土地利用方式下土壤持水能力的差异。结果表明:自然生态系统土壤性质优于人工生态系统,灌草地和玉米地土壤理化性质、分形维数和酶活性分别优于同系统中其他土地利用方式;自然生态系统土壤持水能力大于人工生态系统,自然生态系统土壤持水特征均表现为灌草地>撂荒地>自然林,人工生态系统土壤持水特征均表现为玉米地>人工林>核桃林>猕猴桃;相关性分析结果表明,容重、总孔隙度、有机质含量、颗粒组成和土壤酶活性均会对土壤持水产生影响;主成分分析结果表明,黏粒、砂粒、蔗糖酶、脲酶、磷酸酶、脱氢酶、饱和持水量和毛管持水量对土壤持水能力的累积贡献率高达83.901%。为提高峰丛洼地石漠化区土壤的持水能力,对于人为扰动较小的撂荒地、灌草地、人工林和自然林,应减少人为扰动;对于人为扰动较大的玉米地、核桃林和猕核桃,应该减少人为扰动、提高植被盖度。灌草地可以作为峰丛洼地石漠化区修复治理过程中优先考虑的土地利用方式。

     

    Abstract: The purpose of exploring the differences in water holding capacity of surface soil and the factors affecting it under different land uses in the peak cluster depression of the rocky desertification area is to improve the water holding capacity of its soil. In this study, three natural ecosystem land use modes (abandoned land, shrub land and natural forest) and four artificial ecosystems (artificial forest, Zea mays land, Juglans regia forest, and Actinidia chinensis) were taken as the objects of the study, and the characteristics of soil water-holding indexes (maximum water holding capacity, capillary water holding capacity and field water holding capacity) and soil properties were measured to investigate the differences in soil water-holding capacity among different land use modes of the peak cluster depression of the rocky desertification area. The results showed that (1) the soil properties of natural ecosystems were better than those of artificial ecosystems. In particular, the soil physico-chemical properties (bulk density, porosity and organic matter), fractal dimension and enzyme activity of the irrigated grassland and maize land were better than those of the other land uses in the system, respectively. (2) Natural ecosystem had a greater water-holding capacity than artificial ecosystem. The soil water-holding characteristics of natural ecosystem all showed shrub land>abandoned land>natural forest; the soil water-holding characteristics of artificial ecosystem all showed Zea mays land>artificial forest> Juglans regia forest>Actinidia chinensis. (3) The results of correlation analysis showed that the bulk density, the total porosity, organic matter content, particle composition and soil enzyme activities all affect soil water-holding; and the results of principal component analysis showed that the cumulative contribution of clay, sand, sucrase, urease, phosphatase, dehydrogenase, maximum water holding capacity and capillary water holding capacity to soil water-holding capacity was 83.901%. In order to improve the water-holding capacity of the soil in the peak cluster depression of the rocky desertification area, man-made disturbance should be reduced in disturbed abandoned land, shrub land, artificial forests and natural forests, which have less man-made disturbance; and man-made disturbance should be reduced in the case of Zea mays land, Juglans regia forest and Actinidia chinensis, which had more man-made disturbance, on the one hand, and vegetation cover can be increased on the other hand. On the whole, in the process of restoration and management of rocky desertification areas in the peak cluster depression, shrub land can be the preferred land use mode.

     

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